The Beaded Burial central to F101 within Cahokia’s mound 72Sub1 has been fundamental to some cosmological explanations of the founding of this North American precolumbian polity. The central burial, identified as two males surrounded by retainers, has been interpreted as paradigmatic of a paramount chiefdom, or conversely, as a mythic cosmogram. Recent bioarchaeological reanalysis and two independent osteological studies of F101 and associated burials have identified the presence of male/female pairs, numerous females, and at least one child, suggesting that previous explanations privileging the male Red Horn association should be reexamined. We suggest that 72Sub1 is most likely correlated with ritual practices promoting world creation, renewal, and fertility symbolism.

Discussions of polydactyly in the U.S. Southwest describe rock art and skeletal material confirming the presence of six-toed individuals at a variety of sites and in a variety of time periods. A review of Pueblo Bonito collections and archives reveals both skeletal and footprint evidence for six-toed individuals and a large and diverse assemblage of cultural material exhibiting foot-related imagery, including ornaments, sandals, ceramic effigies, and sandal-shaped ground stone. The reiterative nature of these foot-related images, reproduced in a wide range of media, and their frequent associations with highly structured and ritualized contexts, indicates that both five- and six-toed feet had symbolic importance. The evidence also suggests six-toed individuals were accorded special status within Chacoan society.

Recent archaeological investigations at Pueblo Bonito in Chaco Canyon reveal that residents constructed a large diversion channel during the eleventh century A.D. as dramatic growth resulted in the expansion of the building onto the main valley floor. Sediments in the diversion channel reflect repeated episodes of flooding, rather than slow moving water typically found in irrigation canals, and archaeobotanical data indicate deposition during late summer or early fall. Although an agricultural function is possible, the channel may have been built primarily to divert floodwaters away from Pueblo Bonito while providing a nearby water source for construction and domestic use. The diversion channel was destroyed by the entrenchment of the “Bonito paleo-channel” in the late A.D. 1000s, and then buried by a combination of cultural debris and valley flooding. Although the canyon stream system changed throughout the occupation of Pueblo Bonito, there is no evidence that the formation of a deep natural channel in the floodplain had any negative effect on the growth of the great house

In 1997, Alison Wylie outlined an epistemic and ontological critique of archaeological inquiry to advance feminist science studies. Wylie’s work, I argue, remains relevant and potentially transformative for analysis of the cultural florescence that took place in Chaco Canyon, New Mexico, during the ninth through twelfth centuries A.D. Archival, archaeological, and ethnographic data presented here suggest that women had important and undertheorized roles to play in the social transformations that defined emergent Chacoan society. Legacy data made available through the Chaco Research Archive provide evidence in support of Lamphere’s (2000) ritual power model interpretation of the Chacoan florescence. The advent of such open-access resources allows for a critical analysis of gender ideologies and praxis through aggregated legacy sources that augment analyses based on surviving, institutionally curated artifact collections and published sources.

Although the Great Basin of North America has produced some of the most robust and ancient fiber artifact assemblages in the world, many were recovered with poor chronological controls. Consequently, this class of artifacts has seldom been effectively incorporated into general discussions of early chronological and cultural patterns. In recent years, the Great Basin Textile Dating Project has accumulated direct AMS dates on textiles (bags, sandals, mats, cordage, and basketry) from dry caves in the Great Basin, particularly in the northern and western areas. We focus here on the terminal Pleistocene/early Holocene, to identify chronological patterns in this class of artifacts and to evaluate Adovasio’s characterization of the region’s earliest basketry as simple and undecorated. New AMS dates now suggest that the region’s earliest people had sophisticated textile traditions that incorporated numerous decorative elaborations. Some distinctive structures, including Fort Rock sandals and weft-faced plaited textiles, have limited early temporal ranges and may serve as diagnostic indicators for terminal Pleistocene/early Holocene times. Other basketry forms and structures that appear by about 9000 cal B.P. persist into the historic period, suggesting a stronger thread of continuity (especially in the north) from this time than is apparent in lithic traditions

Following the entry of Zea mays to northeast North America, Northern Iroquoian populations expanded their numbers and range. Isotopic values from bone collagen have shown fluctuations in reliance on this dietary staple. With permission of the Huron-Wendat Nation of Wendake, Quebec, we measured δ13Cenamel, δ13Cdentine and δ15Ndentine from 167 permanent teeth, retained before reburial of their ancestral skeletons, and δ13Ccollagene and δ15Ncollagene from adhering bone (n = 53). Enamel values encapsulate diet from ca. 1.5 to 4 years of age; dentine values reflect later childhood. Teeth are from 16 ancestral Huron-Wendat sites in southern Ontario. Isotopic values show consistent reliance on maize from early fourteenth to sixteenth centuries, with higher reliance in the seventeenth century—the time of contact with Europeans and disruptive changes. We show a difference between the diets of children and adults; children consumed more maize and less animal protein. Whitetailed deer (Odocoileus virginianus) did not exploit maize fields, reflecting hunters’ exploitation of distant regions. New values from fish species (n = 21) are pooled with prior data, demonstrating diverse C and N stable isotope patterns. American eel (Anguilla rostrata) is particularly variable. Dietary protein sources were variable compared to the stability of maize: a reliable source of carbohydrate food energy across four centuries.

As federally and non-federally recognized tribal communities assert control over the management of tribal heritage, there is a significant opportunity to work with these nations to further refine and develop approaches to archaeological practice that work for the long-term care and protection of tribal heritage. This article evaluates the methodological implications of integrating indigenous values and cultural protocols into archaeological practice and tribal historic preservation. Drawing upon the example of the Kashaya Pomo Interpretive Trail Project at Fort Ross State Historic Park, I examine how respectful, engaged, community-based dialogue with the Kashia Band of Pomo Indians led to the development of a lowimpact archaeological methodology that contributes to the capacity of the Kashia Tribal Historic Preservation Office (THPO) to employ archaeology as a tool of historic preservation. Although this methodology was developed with specific reference to the needs and cultural protocols of the Kashaya Pomo, it provides a salient model of a sovereignty-based approach to tribal historic preservation that may be relevant to other tribal heritage managers. The application of a suite of low-impact survey methods, including the catch-and-release surface collection strategy, also provides tribal and nontribal heritage professionals with additional tools for recovering data from cultural resources with minimal impact.

Beads manufactured from marine shells originating along the Pacific Coast have been found at numerous sites in the western United States. Because they were conveyed across substantial distances and widely exchanged during ethnographic times, researchers generally assume that shell beads were also traded prehistorically. By examining the spatial and temporal distribution of beads, researchers have reconstructed prehistoric exchange networks. In this article, we present stable isotope data and accelerator mass spectrometer (AMS) radiocarbon dates for six Callianax (previously Olivella) biplicata beads from the LSP-1 rockshelter in southcentral Oregon. Most of the beads were deposited during the early Holocene during a series of short-term occupations and the shells used to manufacture them were procured along the northern California, Oregon, or Washington coasts.

Studies have long noted the influence of stone package size and reduction intensity on lithic assemblage composition, particularly in the form of flake size distributions. However, it remains difficult to distinguish objectively the effect of either factor in archaeological contexts without controlling for the variation in one of the two variables. Here we report on an experimental study designed to test the null hypotheses that original stone size and reduction intensity have no impact on the size distribution of lithic flake debris produced during core reduction. Results indicate statistically significant influence from original stone size but not reduction intensity, although the effects from the former are low enough to be considered trivial. In reviewing a sequence of archaeological assemblages from a Middle Paleolithic site, all exhibit an excess of smallsized materials in comparison to the experimental data. When exceptionally high frequencies of the smaller size classes occur, taphonomic processes are clearly responsible.

Human culture signifies the emergence of an entirely new domain of existence: an event in natural history that is paralleled only by the Cambrian Explosion in terms of creativity and scope. The question of how human culture—as opposed to its animal counterparts—came to become open-endedly creative and cumulative is therefore one of wide and general scientific importance. Several causal factors have been proposed to date to explain this unique quality, including population size, transmission fidelity, pedagogy, and creativity. Inquiries, however, tend to focus exclusively on one factor at a time, leaving us blind to important issues regarding their relative roles and combined action. We here combine two models, one focusing on population size and the other on imitation fidelity, as constraints and enablers of evolutionary cumulativity. We explore how these factors interact to promote and inhibit evolutionary cumulativity and how the synthetic model compares to the original models individually and to empirical and experimental data. We report several findings that do not emerge in the models that we combine individually. For example, group size is found to be important for small but not for larger groups, an observation that moreover substantially improves agreement with data.

Glassow’s (2015) synthesis of “red abalone middens” on California’s Santa Cruz Island does not include the broader geographic, chronologic, and ecological context to this phenomenon. We explore the wider distribution of these site types and emphasize their importance for addressing modern fisheries management issues.

Although Braje and Erlandson express concern with my inclusion of Santa Cruz Island sites containing small quantities of red abalone shells with red abalone middens on the other Channel Islands, doing so is justified because of the discrete period of time during which they occur. They also feel that I should have expanded the scope of my paper to include consideration of relationship between sea otters and red abalone, but this was beyond the intent of my report. Nonetheless, I point out that more explication is needed of the nature of sea otter hunting if its effects on red abalone availability are to be understood.